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arXiv 2510.00596astro-ph.SR
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由m=1高纬度惯性模引起的太阳光球磁场振荡

Oscillations of the solar photospheric magnetic field caused by the m = 1 high-latitude inertial mode

Stephan G. Heinemann, Zhi-Chao Liang, Laurent Gizon

AI总结:

本研究利用HMI和GONG的长期磁图序列,检测到地球参考系中高纬度(65°--70°)存在频率为338 nHz的周期性磁场振荡,其特征与m=1高纬度惯性模一致,为该模式的光球磁场响应提供观测证据。

摘要:

在地球参考系中,通过直接多普勒速度测量观测到高纬度地区存在频率为338 nHz的周期性振荡,这些振荡对应于m=1高纬度全局惯性振荡模。本研究利用太阳动力学观测台的日震和磁像仪(HMI)及全球振荡网络组(GONG)的长期视向磁图序列,研究该模式在光球磁场中的特征。通过直接观测和频谱分析,我们在地球参考系中检测到高纬度(65°--70°)存在频率为338 nHz的周期性磁场振荡,与已知的m=1高纬度惯性模频率匹配。观测到的视向磁场振荡在赤道两侧主要呈对称分布。我们发现磁场振荡峰值振幅高达0.2高斯,且具有明显的空间模式,这两者均与简化模型计算结果一致,该模型中磁场的径向分量被模式的水平流场平流输送。

英文摘要:

Periodic oscillations at 338 nHz in the Earth frame are observed at high latitudes in direct Doppler velocity measurements. These oscillations correspond to the $m=1$ high-latitude global mode of inertial oscillation. In this study, we investigate the signature of this mode in the photospheric magnetic field using long-term series of line-of-sight magnetograms from the Helioseismic and Magnetic Imager (HMI) and the Global Oscillation Network Group (GONG). Through direct observations and spectral analysis, we detect periodic magnetic field oscillations at high latitudes ($65^\circ$--$70^\circ$) with a frequency of 338 nHz in the Earth frame, matching the known frequency of the $m = 1$ high-latitude inertial mode. The observed line-of-sight magnetic field oscillations are predominantly symmetric across the equator. We find a peak magnetic oscillation amplitude of up to $0.2$~gauss and a distinct spatial pattern, both consistent with simplified model calculations in which the radial component of the magnetic field is advected by the mode's horizontal flow field.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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